<p>(a) The gray diamond and blue circle indicate the landslide inventories of the Guatemala and Taiwan case. The red line is the reference distribution with ρ = 1.4, <i>a</i> = 1.28×10<sup>−3</sup> km<sup>2</sup>, <i>s</i> = 1.32×10<sup>−4</sup> km<sup>2</sup>. The solid and dashed yellow lines represent the distribution with 0.8ρ and 1.2ρ, respectively. Their corresponding <i>r</i><sup>2</sup> to the reference reach 0.973 and 0.976, respectively. (b) Change of total area and large landslide proportion is associated with the change of the exponent.</p
This paper presents a new methodology to systematically quantify the shape of landslides by their el...
Abstract. We examine 19 datasets with measurements of landslide volume, VL, for sub-aerial, submarin...
The standard definition of landslide hazard requires the estimation of where, when (or how frequentl...
[[abstract]]The exponent decay in landslide frequency-area distribution is widely used for assessing...
[[abstract]]Landslide is a catastrophic disaster over the world, which leads to sediment-associated ...
Landslides are generally associated with a trigger, such as an earthquake, a rapid snowmelt or a lar...
This paper relates landslide inventories to erosion rates and provides quantitative estimates of the...
Discovering the physical explanations behind the power-law distribution of landslides can provide va...
<p>The green and blue dots are produced by NLB with b = 0.1 and 0.5, respectively. The red lines are...
Summary statistics derived from the frequency–area distribution (FAD) of inventories of triggered la...
Earthquake-Induced Landslide (EQIL) inventories are the key to improve our understanding of the rela...
A power‐law relation for the frequency‐area distribution (FAD) of medium and large landslides (e.g.,...
Statistical methods are commonly employed to estimate spatial probabilities of landslide release at ...
As the global climate changes, the threat from landslides and debris flows increases. Learning how a...
We examine 19 datasets with measurements of landslide volume, <I>V<sub>L</sub><...
This paper presents a new methodology to systematically quantify the shape of landslides by their el...
Abstract. We examine 19 datasets with measurements of landslide volume, VL, for sub-aerial, submarin...
The standard definition of landslide hazard requires the estimation of where, when (or how frequentl...
[[abstract]]The exponent decay in landslide frequency-area distribution is widely used for assessing...
[[abstract]]Landslide is a catastrophic disaster over the world, which leads to sediment-associated ...
Landslides are generally associated with a trigger, such as an earthquake, a rapid snowmelt or a lar...
This paper relates landslide inventories to erosion rates and provides quantitative estimates of the...
Discovering the physical explanations behind the power-law distribution of landslides can provide va...
<p>The green and blue dots are produced by NLB with b = 0.1 and 0.5, respectively. The red lines are...
Summary statistics derived from the frequency–area distribution (FAD) of inventories of triggered la...
Earthquake-Induced Landslide (EQIL) inventories are the key to improve our understanding of the rela...
A power‐law relation for the frequency‐area distribution (FAD) of medium and large landslides (e.g.,...
Statistical methods are commonly employed to estimate spatial probabilities of landslide release at ...
As the global climate changes, the threat from landslides and debris flows increases. Learning how a...
We examine 19 datasets with measurements of landslide volume, <I>V<sub>L</sub><...
This paper presents a new methodology to systematically quantify the shape of landslides by their el...
Abstract. We examine 19 datasets with measurements of landslide volume, VL, for sub-aerial, submarin...
The standard definition of landslide hazard requires the estimation of where, when (or how frequentl...